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浦市铜矿地质特征及成矿地质条件初探
引用本文:官鹏程,梁惠敏,陈明辉,周旭林,徐军伟,鲍振襄,包觉敏.浦市铜矿地质特征及成矿地质条件初探[J].地质找矿论丛,2016,31(2):199-205.
作者姓名:官鹏程  梁惠敏  陈明辉  周旭林  徐军伟  鲍振襄  包觉敏
作者单位:1. 湖南省有色地质勘查局二四五队,湖南 吉首,416007;2. 湖南省有色地质勘查局二四五队,湖南 吉首 416007;中南大学地球科学与信息物理学院,长沙 410083;3. 湖南省地质科学研究院,长沙,410007;4. 湖南省有色地质勘查局二四七队,长沙,410129;5. 湘西矿产资源综合研究发展中心,湖南 乾州,416009
摘    要:文章在阐述浦市铜矿床地质特征的基础上,初步探讨了矿床的成矿地质条件。矿床赋存于下白垩统紫红色碎屑岩夹灰白-灰绿色砂岩中,其成矿物质主要来自陆缘;矿床形成于氧化态向还原态过渡的沉积环境,在其沉积成岩和成矿过程中都有生物地球化学作用,属沉积砂岩型铜矿床。

关 键 词:浦市铜矿  地质特征  成矿地质条件  沉积砂岩型矿床  湖南省
收稿时间:2015/2/11 0:00:00
修稿时间:2016/1/22 0:00:00

Geological characteristics and metallogenic conditions of Pushi copper deposit
GUAN Pengcheng,LIANG Huimin,CHEN Minghui,ZHOU Xulin,XU Junwei,BAO Zhenxiang and BAO Juemin.Geological characteristics and metallogenic conditions of Pushi copper deposit[J].Contributions to Geology and Mineral Resources Research,2016,31(2):199-205.
Authors:GUAN Pengcheng  LIANG Huimin  CHEN Minghui  ZHOU Xulin  XU Junwei  BAO Zhenxiang and BAO Juemin
Institution:Hunan Non-ferrous Metals Geology Investigation Bureau Rows 245, Jishou 416007, Hunan, China;Hunan Non-ferrous Metals Geology Investigation Bureau Rows 245, Jishou 416007, Hunan, China;Hunan Non-ferrous Metals Geology Investigation Bureau Rows 245, Jishou 416007, Hunan, China;School of Geosciences and Info-Physics, Central South University, Changsha 410083, China;Department of Land and Resources of Hunan Province, China, Changsha 410004, China;Team 247 of Hunan Provincial Nonferrous Metals Geological Exploration Bureau, Changsha 410129, China;Xiangxi Mineral Resources Research and Development Center, Qianzhou 416009, Hunan, China;Xiangxi Mineral Resources Research and Development Center, Qianzhou 416009, Hunan, China
Abstract:Based on geological characteristics of Pushi copper deposit the metallogenic conditions are discussed. It occurs in Lower Cretaceous purple clastic rock intercalated with grey white to grey green sandstone and ore materials come from continent. It is formed under transitional environment from oxidation to reduction and bio-geochemical process is involved. It is a sedimentary sandstone type copper deposit.
Keywords:Pushi copper deposit  geological characteristic  metallogenic condition  sedimentary sandstone type deposit  Hunan province
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